Vermiculite from pegmatitic phlogopitic gabbro, Central Turkey.

Date

2000-06-29

Author

Toksoy Köksal, Fatma
Göncüoğlu, M. Cemal

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https://hdl.handle.net/11511/84823

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Vermiculitization of phlogopite in Metagabbro, central Turkey Toksoy Köksal, Fatma; Göncüoğlu, Mehmet Cemal (2001-02-01) Dioctahedral vermiculite occurs in an isolated metagabbro klippe (Kurancali Metagabbro) that belongs to the Central Anatolian Ophiolites from central Turkey. Both the metagabbro and the structurally underlying high-grade metamorphic rocks are intruded by granitic rocks. The Kurancali Metagabbro is characterized by its well-developed compositional layering, and the presence of vermiculitized phlogopite rich layers. Petrographic and mineralogic studies show that the primary mineral phases in the host rock are...
Vermiculitization of phlogopites within metagabbro, Central Turkey Toksoy Köksal, Fatma; İçöz, Serap; Göncüoğlu, M. Cemal (null; 1999-09-09)
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Pyrolysis characteristics of Turkish lignites in N-2 and CO2 environments BARZEGAR, RAMİN; Avşaroğlu, Sevil; Yozgatlıgil, Ahmet; Atımtay, Aysel (2018-01-01) Pyrolysis characteristics and kinetic parameters of two Turkish lignites having different ash contents (Orhaneli as low ash and Soma as high ash sample) were studied under N-2 and CO2 atmospheres by means of thermogravimetric analysis. The isoconversional kinetic methods of FlynnWallOzawa, KissingerAkahiraSunose, and Friedman were employed to estimate the activation energy and pre-exponential factors. The experiments were conducted at four different heating rates of 5, 10, 15, and 20 degrees C/min within th...

Citation Formats

F. Toksoy Köksal and M. C. Göncüoğlu, “Vermiculite from pegmatitic phlogopitic gabbro, Central Turkey.,” 2000, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/84823.